氮磷添加对湿地松人工林土壤有机碳组分的影响
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S714

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国家重点研发计划项目(2017YFD0600502)和安徽省自然科学基金项目(1908085MC73)资助。


Effects of Nitrogen and Phosphorus Addition on Soil Organic Carbon Fraction in Pinus elliottii Plantation
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National Key Research and Development Program of China(2017YFD0600502); Anhui Provincial Natural Science Foundation(1908085MC73)

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    摘要:

    本文以安徽省宣城市宛陵林场湿地松林为研究对象,通过设置对照(CK, N 0 kg/(hm2·a)+P 0 kg/(hm2·a))、低氮(LN, N 50 kg/(hm2·a)+ P 0 kg/(hm2·a))、高氮(HN, N 100 kg/(hm2·a)+ P 0 kg/(hm2·a))、高氮低磷(HNLP, N 100 kg/(hm2·a)+P 50 kg/(hm2·a))和高氮高磷(HNHP, N 100 kg/(hm2·a)+P 100 kg/(hm2·a))5种处理,开展连续5年的野外氮磷添加控制试验,并于2023年测定0~20、20~40 cm土层土壤基本性质、有机碳组分和水解酶活性,探究了短期氮磷添加对森林土壤有机碳组分含量的影响及其关键因素。结果表明:①氮磷添加下,土壤pH显著降低了3.49%~11.48%,HNLP处理下0~20 cm土层土壤硝态氮、全磷含量分别显著增加了128.10%、76.67%;②5年氮添加对土壤有机碳(SOC)、颗粒态有机碳(POC)、矿物结合态有机碳(MAOC)、微生物生物量碳(MBC)含量无显著影响,HN处理下土壤可溶性有机碳(DOC)含量显著提高,HNLP处理下0~20 cm土层SOC、POC、MAOC含量分别显著增加了31.51%、18.01%、27.12%,20~40 cm土层MBC含量显著增加了13.35%;③结构方程模型表明,氮磷添加改变了土壤中硝态氮和全磷含量,通过直接或者间接影响土壤β-1, 4-葡萄糖苷酶、纤维二糖苷酶、β-1, 4-N-乙酰葡糖氨糖苷酶活性来影响土壤碳组分含量。因此,从长期碳固持的角度来看,高氮低磷混合施用模式更有利于提高土壤有机碳的稳定性。该研究结果为森林“双碳”目标的实现提供了森林经营理论支持。

    Abstract:

    In this study, the Pinus elliottii plantation in Wanling Forest Farm, Xuancheng City, Anhui Province was selected as the research object. A controlled field nitrogen (N) and phosphorus (P) addition experiment was conducted with five treatments, including control check (CK, N 0 kg/(hm2·a)+P 0 kg/(hm2·a)), low N (LN, N 50 kg/(hm2·a)+P 0 kg/(hm2·a)), high N (HN, N 100 kg/(hm2·a)+P 0 kg/(hm2·a)), high N and low P (HNLP, N 100 kg/(hm2·a)+P 50 kg/(hm2·a)) and high N and high P (HNHP, N 100 kg/(hm2·a)+P 100 kg/(hm2·a)). Based on five consecutive years of controlled experiments with N and P additions, basic soil properties, organic carbon fractions and hydrolytic enzyme activities of 0-20 cm and 20-40 cm soil layers were measured in 2023, to explore the effects of short-term N and P addition on soil organic carbon(SOC) fraction contents and their key influencing factors. The results showed that: 1) The addition of N and P significantly decreased soil pH by 3.49%-11.48%, and HNLP significantly increased the contents of NO- 3-N and total P respectively by 128.10% and 76.67%. 2) N addition of 5 years had no significant effect on the contents of SOC, particulate organic carbon(POC), mineral-associated organic carbon(MAOC) and microbial biomass carbon(MBC), while HN significantly increased the content of dissolved organic carbon(DOC). HNLP significantly increased the contents of SOC, POC and MAOC in 0-20 cm soil layer by 31.51%, 18.01%, and 27.12%, respectively, and significantly increased the content of MBC in 20-40 cm soil layer by 13.35%. 3) Structural equation model analysis showed that N and P addition changed the contents of NO- 3-N and total P in soil, affected soil carbon fractions by directly or indirectly affecting soil β-1,4-glucosidase, cellobisidase, β-1, 4-N-acetylglucosaminidase activities. Thus, from the perspective of long-term carbon sequestration, the mixed use of high N and low P is more beneficial to improve the stability of soil organic carbon, which provides theoretical support for forest management to realize the goals of forest carbon peaking and carbon neutrality.

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何徽,李威,马溯,张愁愁,刘艺,刘西军.氮磷添加对湿地松人工林土壤有机碳组分的影响[J].土壤,2026,58(2):346-353. HE Hui, LI Wei, MA Su, ZHANG Chouchou, LIU Yi, LIU Xijun. Effects of Nitrogen and Phosphorus Addition on Soil Organic Carbon Fraction in Pinus elliottii Plantation[J]. Soils,2026,58(2):346-353

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  • 收稿日期:2024-12-02
  • 最后修改日期:2025-01-25
  • 录用日期:2025-02-14
  • 在线发布日期: 2026-05-09
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